siberian and canadian
Water fountains that produce two streams of water allows the customer to drink more water with less air, therefore less burping. Also with two streams there is less spraying.
Lewis L DeLong has written: 'An analysis of salinity in streams of the Green River Basin, Wyoming' -- subject(s): Salinity
Freshwater biomes, such as rivers, streams, lakes, and ponds, typically have a salinity of 0.005 or less. These bodies of water contain very low levels of dissolved salts compared to marine or estuarine environments.
Coastal waters have a lower salinity due to the vast amount of freshwater runoff pouring into the sea from rivers and streams. PM
The two main processes that contribute to high salinity rates in water bodies are evaporation and lack of freshwater input. When water evaporates, salts are left behind, increasing the salinity of the remaining water. Without enough freshwater input to dilute the salt content, salinity levels can continue to rise.
deep canyons
When two streams come together, it is called a confluence. At a confluence, the two streams merge to form a single stream.
There are several factors that the Red Sea has high salinity. The Red Sea has a high rate of evaporation and very little precipitation. It also has a limited connection with the Indian Ocean, which has lower water salinity. The Red Sea has a lack of significant rivers or streams draining into the sea.
Ocean currents,The sun,and human activities
Salinity is generally lowest in areas where freshwater sources like rivers and streams meet the ocean, such as estuaries and deltas. Other factors like heavy rainfall and melting ice can also contribute to lower salinity levels in certain regions.
Well there may be more than two. The rivers flow into the sea, thus diluting the salt, but salt carried by the river will increase the salt content. Salt may be removed by precipitation, but only if the concentration becomes great.